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The main consequence of the ozone depletion, which is apparent over much of the globe several yeas ago, is the increase of the biologically damaging UV irradiance at the ground level. Data for the airborne spectral observations of upward irradiance at the upper level (∼5 km) and downward irradiance at the down level (∼500m) are compared for finding the empirical dependence between them. Radiation experiments aver different surfaces (sand, water, snow) and in different conditions (clear or cloudy sky) are considered.
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